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CIE 0625 Physics · IGCSE · Topic 1.8

Pressure

Clear, syllabus-mapped CIE 0625 Physics revision notes on pressure: explanations, worked examples and exam technique, then a free targeted practice drill.

CIE 0625 PhysicsIGCSEFree revision notes
Contents: 7 sections

Cambridge IGCSE Physics 0625 · Core and Extended

Syllabus points

The equation

pressure = force / area

p = F/A, in N/m² (pascals) or N/cm².

The force pressing on a surface is the weight of whatever rests on it, in newtons. Mass in kilograms is not a force and does not belong in this equation.

Because the area is on the bottom:

Skis and snowshoes work by making the area large so the pressure stays low enough not to sink. A drawing pin and a knife blade work the other way, concentrating a modest force onto a tiny area.

Worked example. A skier weighs 550 N and his skis touch the snow over 0.015 m².

p = 550 / 0.015 = 36 667 N/m², which to two significant figures is 37 000 N/m².

Dividing by a number smaller than one makes the answer bigger, so any option below 550 can be discarded on sight.

Choosing the right face

When a block can rest on different faces, the weight does not change but the contact area does.

The word "least" tempts people towards the smallest face. Least pressure needs the greatest area.

For a block 40 cm by 20 cm by 80 cm, the three faces are 3200 cm², 1600 cm² and 800 cm². Reading the diagram to see which dimensions form the base is the whole question, and papers often give a separate option for each wrong pairing of two dimensions.

Worked example. A block 1 m by 1 m by 5 m weighs 125 000 N. What happens to the pressure if it is stood on its end rather than laid on its long side?

Lying down: base = 1 x 5 = 5 m², so p = 125 000 / 5 = 25 000 N/m². Stood up: base = 1 x 1 = 1 m², so p = 125 000 / 1 = 125 000 N/m². Change = an increase of 100 000 N/m².

Note the question asks by how much the pressure changes, not what it becomes.

Pressure in a liquid

p = h ρ g

where h is the depth below the surface, ρ the density and g the gravitational field strength. The depth must be in metres.

Only three things appear in that expression, and the consequences are worth stating plainly:

A narrow tube and a wide tank filled to the same depth press equally hard at the bottom. A reservoir behind a dam presses on the wall according to depth alone, not the length of the lake behind it. This feels wrong the first time and is a favourite question.

Pressure at a point in a liquid also does not depend on the object sitting there. Changing a stone's mass or surface area changes nothing about the pressure the liquid exerts on it.

Worked example. A column of liquid 50 cm deep produces a pressure of 6000 N/m² at the bottom. Find its density.

h = 0.50 m. ρ = p / (g h) = 6000 / (10 x 0.50) = 1200 kg/m³.

Failing to convert 50 cm to metres makes the answer a hundred times too large, and the result would then be denser than any material on Earth.

Change in pressure depends only on the change in depth. Two submarines each descending 20 m experience the same change, however deep each one started.

Manometers

A U-tube of liquid, open to the air at one end and connected to a gas supply at the other. The difference between the two levels measures how far the gas pressure differs from atmospheric.

The reading is always the difference between the levels, never a single level.

The direction follows from which side is lower:

Where a manometer holds two liquids over mercury and the mercury levels are equal, the pressures on the mercury from each side must be equal. If one column is taller and they balance, the taller liquid must be the less dense, since p = hρg.

Barometers

A mercury barometer is a tube closed at the top, filled with mercury and stood in a dish. There is a vacuum above the mercury in the tube.

The atmospheric pressure is measured by the vertical height of mercury above the level in the dish.

Three things are easy to get wrong.

Narrowing the tube changes nothing either. A wider tube holds more mercury but spreads its weight over proportionally more area.

Mercury is used because it is dense. A water barometer would need a column over ten metres tall to balance the same atmosphere.

Within the mercury, pressure follows the same rule as any liquid: it is near zero in the vacuum, below atmospheric part way up the column, atmospheric at the surface in the dish, and above atmospheric anywhere below that surface.

Common mistakes

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